https://acp.copernicus.org/articles/26/523/2026/

*Authors: *Ehsan Erfani and David L. Mitchell

*12 January 2026*

*Abstract*
The efficacy of the climate intervention method known as cirrus cloud
thinning (CCT) is difficult to evaluate in climate models, largely due to
uncertainties governing the relative contributions of homogeneous and
heterogeneous ice nucleation. Here we take a different approach by
employing recent satellite retrievals from the Cloud-Aerosol Lidar and
Infrared Pathfinder Satellite Observation (CALIPSO) which provide estimates
of the fraction of cirrus clouds dominated by homogeneous and heterogeneous
ice nucleation and their associated physical properties. We employ a
radiative transfer model (RTM) to quantify the cloud radiative effect for
homogeneous and heterogeneous cirrus clouds at the top of atmosphere (TOA),
Earth's surface, and within the atmosphere. The RTM experiments are
initialized using cirrus microphysical profiles derived from CALIPSO
retrievals for cirrus clouds dominated by homogeneous and heterogeneous ice
nucleation across different regions (Arctic, Antarctic, and midlatitude)
and surface types (ocean and land). We define two bounds: the lower bound
assumes a full microphysical transition from the observed composition of
homogeneous- and heterogeneous-dominated cirrus to only heterogeneous
cirrus and production of new cirrus. The upper bound assumes production of
new cirrus and that the atmospheric dynamics enables homogeneous freezing
nucleation to occur regardless of the concentration of ice nucleating
particles. Based on these bounds, we estimate an instantaneous surface
effect ranging from −0.5 to +0.6 W m−2 and a TOA effect from −0.9 to +1.1 W
m−2, respectively, showing the possibility of both cooling and warming.
Recommendations are provided to improve the treatment of cirrus clouds in
climate models.

*Source: EGU*

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